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Air Flow Optimization for Remediation using SPARG Diane Fink Liz Hilkert.

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Presentation on theme: "Air Flow Optimization for Remediation using SPARG Diane Fink Liz Hilkert."— Presentation transcript:

1 Air Flow Optimization for Remediation using SPARG Diane Fink Liz Hilkert

2 Significance and Objective  Optimal airflow rates are important in remediation –Ensure maximum contaminant volatilization –Prevent channeling  Determine ideal capillary pressures for a one meter soil column –varying water table heights

3 SPARG Information  Unix based program for one or two dimensional column simulations  Uses finite element-Galerkin's formulation  The airflow simulation model that is the basis for AirFix –Includes contaminant transport

4 SPARG Calibration  Only dependable data from 2D model  Capillary Head of 10.15 m  Calibration successful

5 Sensitivity Analysis Sensitive Variables Capillary PressureSaturation Atmospheric PressureAll Soil Lambda PorosityAve Saturation Sensitivity 0.3400.109Min-Def1.003 0.3900.125Def-Max0.998 0.4400.141 Atmospheric Pressure Capillary Pressure at Y =0.4 Sensitivity 8.000-0.524Min-Def29.032 10.0000.276Def-Max6.509 12.0001.076

6 SPARG Inputs  Constant Inputs: –Psubd: 0.2 m –Soil Lambda: 3.4 –Porosity: 0.39 –Grid: 1,10 –Grid Division: 0.1 m –Atmospheric Pressure: 10 m 20 elements 22 nodes

7 Varied SPARG Inputs  Water Table Height: –Half of Sand Height: 0.33 m –Full Sand Height: 0.67 m  Airflow Entry Rate (nodes 1 and 2): –Varied by increasing air entry pressure –Minimum for half full: 10.53 m –Minimum for full: 10.87 m

8 Effect of Air Entry Pressure at Full Water Table Height (0.67 m) Saturation Capillary Pressure

9 Effect of Air Entry Pressure at Half Water Table Height (0.33 m) Capillary Pressure Saturation

10 Graphical Trends  Capillary pressure: –linear relationship with column height –indirectly proportional to water table height –directly proportional to air entry pressure at lower water table heights  pressures converge as air reaches the top of the column, which is atmospheric  Saturation: –nonlinear relationship with column height –directly proportional to water table height –indirectly proportional to air entry pressure at lower water table heights  saturation levels converge as air reaches the top of the column, which is atmospheric

11 Conclusions  Full Water Table Height (0.67 m): –Air entry pressure range: 10.871 – 10.89 m  Half Water Table Height (0.33 m): –Air entry pressure range: 10.531 – 10.55 m

12 Thank You Questions?


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